Fractal Dimension Characteristic of Soil Particle-size Distribution in Beijing Region
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Fractal Dimension Characteristic of Soil Particle-size Distribution in Beijing Region
Bulletin of Soiland Water ConservationVol. 29, Issue 2, Pages: 154-158(2010)
作者机构:
北京师范大学地表过程与资源生态国家重点实验室地理学与遥感科学学院,北京,100875
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Published:2010
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GUO Zhong-ling, FU Su-hua, WANG Xiang-liang, et al. Fractal Dimension Characteristic of Soil Particle-size Distribution in Beijing Region[J]. Bulletin of Soiland Water Conservation, 2010, 29(2): 154-158.
DOI:
GUO Zhong-ling, FU Su-hua, WANG Xiang-liang, et al. Fractal Dimension Characteristic of Soil Particle-size Distribution in Beijing Region[J]. Bulletin of Soiland Water Conservation, 2010, 29(2): 154-158.DOI:
Fractal Dimension Characteristic of Soil Particle-size Distribution in Beijing Region
Soil has the fractal characteristic. Soil fractal dimension (SFD) can be used as an important index of soil. In this study
30 soil samples from 7 soil types and 4 landuses were collected. Soil particle-size distribution
soil bulk density
saturated water content
saturated hydraulic conductivity
and soil organic matter were measured. The SFD was then calculated according to soil particle-size distribution. Results showed that the fractal dimension in Beijing region had a low variation coefficient. Significantly positive correlative relationships between the SFD and clay content and between the SFD and saturated hydraulic conductivity were found. The fractal dimension was negatively correlated with the ratio of (sand content + silt content)/clay content. The SFD can be a potential parameter to reflect soil texture
but is not a rational indicator to reflect soil physical properties under complex geographical environment.